subsidence basin 中文意思是什麼

subsidence basin 解釋
沉降池
  • subsidence : n. 1. 沉澱；沉下，陷下。2. 平靜，平息；減退，衰耗。
  • basin : n 1 臉盆；水盆。2 滿盆，（一）盆。3 盆地，流域。4 水坑，地塘；（港灣）深度；內灣，小灣；【造船】...
  1. The study results can be summerized as following aspects : ( 1 ) the basic settling curve of this basin was broken - line shape of seven sections in which upper jurassic, lower cretaceous, eocene, oligocene and neogene corresponded with the decline ones representing five episodic clear subsidences of this basin, late cretaceous to paleocene and early miocene corresponded with the rising ones reflecting the uplift and denudation of this basin. ( 2 ) the subsidence of this basin migrated from the east to the west, from mesozoic to cenozoic

    研究表明： （ 1 ）北黃海盆地的基本沉降曲線型式為7段折線狀，其中晚侏羅世、早白堊世、始新世、漸新世、新近紀為曲線下降段，代表盆地5幕較明顯的沉降；晚白堊世古新世以及中新世早期為曲線上升段，反映盆地的抬升剝蝕。
  2. The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks

    摘要位於班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地，在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側展開的古地理格局：中晚侏羅世時期，裂谷帶內由深水濁積巖、放射蟲硅質巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成；裂谷帶兩側由濱淺海相碎屑巖和碳酸鹽巖組成。
  3. The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution. the basins located in the southern margin of the yangtze plate, in the basin dynamic computer simulation, is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt

    在沉積盆地分析方面，基本查明揚子板塊東南邊緣早古生代被動大陸邊緣沉積特徵及沉積構造演化，同時運用反剝法技術對揚子板塊東南大陸邊緣沉積盆地形成，演化的構造沉降動力學進行探討，運用計算機模擬方法，定量動力沉積學對揚子東南邊緣奧陶紀到志留紀前陸地進行計算機模擬分析，探索並建立這個古老造山帶前陸盆定量參數和動態定量模擬。
  4. One of the frontier recearch of basin analysis in recent years is to analyze the tectonic subsidence history of depositional basins which occur in orogens at different geohistory stage, and to discuss the geodynamic processes involved with the basins

    摘要對造山帶各地史階段的沉積盆地進行構造沉降分析，進而探討其地球動力學過程，是近年來盆地分析的前緣研究之一。
  5. Because of the collision of the terranes, the episodic tectonic activity occurred in the orogenic belt, resulting in the episodic subsidence of the basin

    受地體碰撞的影響，盆地西緣造山帶發生幕式構造運動，從而導致盆地沉降也發生幕式變化。
  6. Compared to the basins in east guangxi, the basin of north guangxi is characterized by lower depositional and tectonic subsidence rate during rifting, longer thermal subsidence, later inflexion point from rifting to foreland buckling, as well as later inflexion point separating stable stage from active stage during foreland - buckling

    但與桂東大瑤山地區相比，桂北興安地區在裂陷階段的沉積速率和構造沉降速率明顯偏低；熱沉降階段的持續時間偏長；裂陷階段與前陸撓曲階段的分界拐點偏晚；前陸撓曲階段，由構造寧靜期的緩慢沉降向構造活動期的快速沉降轉化的分界拐點也偏晚。
  7. Depositional cycles on basin scale have been interpreted as the result of depositional response to tectonism such as episodic rifting, polyphasic compressive flexural subsidence and reversion, and differential subsidence of fault blocks ; while the formation of high frequency sequences was attributed to variation in lake level and sediment supply

    盆地規模的沉積旋迴多是盆地幕式裂陷、多幕擠壓撓曲沉降、多期構造反轉、斷塊差異沉降等構造作用的沉積回應；高頻層序單元的發育則主要與湖平面和沉積物供給量的變化有關。
  8. The general structure of the basin is marked by the tectonic framework of compressional ramp of the east kunlun mountains and the qilian mountains toward and subsidence of the central part of the basin

    盆地的總體結構表現為東昆侖山和祁連山相向向盆地擠壓對沖，盆地中部沉降的構造格局。
  9. Abstract : based on the basic geology this paper determines the development history of kailu basin, and comprehensively analyses hydrogeologic conditions and hydrogeochemical characteristics, as well as the uranium concentration in groundwater, determines the prospecting significance of regional confined aquifers in yaojia and sifangtai formations formed during the subsidence stage of the basin

    文摘:本文從基礎地質條件出發，界定了開魯盆地的發展歷史，全面分析了研究區的水文地質條件、水文地球化學特徵及地下水的含鈾性，確定了在整體坳陷期形成的姚家組和四方臺組區域承壓含水層的找礦意義。
  10. The phase of reservoir formation can be the period when the basin is the subsidence such as the reservoir of shixi 2 well, shi 002 well, shi nan 4 well, cai san 2 well in zhungeer basin, tuo 76 well ; the phase of being reservoir can be the period when the basin is the uplift such as the reservoir of songliao basin, miyang basin, dongpusag, eerduosi basin, yaqi basin

    油氣的成藏期可以在盆地沉降期，如準噶爾盆地石西2井、石002井、石南4井、彩叄2井的油氣藏；也可以在抬升剝蝕期，如松遼盆地、泌陽盆地、東濮凹陷、鄂爾多斯盆地、焉耆盆地的部分油氣藏。
  11. Sequence types and subtle reservoirs exploration in continental rift - subsidence basin

    陸相斷陷盆地層序類型及隱蔽圈閉預測
  12. The different subsidence history not only demonstrates that the two areas have different tectonic settings, but also proves that the caledonian basin migrated to northwest when the cathaysian plate was gradually subducted toward yangtze plate from southeast to northwest

    這些差別這一方面說明了兩地區具有不同的構造背景，另一方面也反映了華夏板塊由南東逐漸地向北西揚子板塊靠攏，沉積盆地相應地向西北遷移的動力學過程。
  13. There are 3 types of reservoir for the continuing subsidence type basin, there are diapir reservoir, fault reservior, drape reservoir, and the source rock is apart from the reservoir, they are contact by fault ; and there are anticline reservoir, fault reservoir, incline reserve ir, mudstone reservoir under the denudation area, and the source rock is contact with the reservoir

    以沉降為主要趨勢的盆地的油氣藏有底辟構造油氣藏、斷層油氣藏、披覆構造油氣藏，其烴源巖與油藏在空間上是分離的，並通過斷層相連；剝蝕區以下的油氣藏有背斜油氣藏或斷層油氣藏、向斜油氣藏及泥質巖油氣藏，其烴源巖和油氣藏可有密切的接觸關系。
  14. The study shows that the basin is subsidenced in the early jurassic period and the sedimentation center lied in tiaohu depression. when it comes to the middle jurassic period, the subsidence center and the sediment center moved to the malang depression. during middle - later jurassic period, the basin subsided stably and the center of sediment and subsidence still lied in malang depression

    表明早侏羅世盆地沉降、沉積中心位於條湖凹陷，中侏羅世盆地沉降中心與沉積中心向東遷移至馬朗凹陷，中晚侏羅世盆地總體表現為穩定、緩慢的沉降，整個盆地的沉積、沉降中心仍在馬朗凹陷。
  15. Bozhong area has different oil - gas accumulation characteristics from the adjace nt onshore oil fields. because of the latter thermal event and tectonic action, bo zhong area became the subsidence center and depo - center of the bohai bay basin

    其具有不同於周邊陸地油田的油氣成藏特點，晚期的熱沉降和構造活動使其成為渤海灣盆地的沉降和沉積中心，上第三系具有優于周邊陸地油田的良好的儲蓋條件，晚期的構造活動與油氣主要排烴期相匹配，為油氣向上第三系圈閉中運聚提供了良好條件。
  16. Through the analysis of subsidence history in the north of western ordos basin, as a result of the terranes northward accretion and the successive collision of the baykala block in the middle triassic, the qiangtang block in the late triassic, the lhasa block in the middle jurassic, the gangdese block in the cretaceous and the subduction of izanagi plate in yanshanian period, the studied region became a intracontinental foreland basin from late triassic to cretaceous

    摘要通過對鄂爾多斯盆地西緣北段沉降史的分析可知，晚三疊世白堊紀，由於中三疊世巴顏喀拉地體、晚三疊世羌塘地體、中晚侏羅世拉薩地塊、白堊紀岡底斯地體連續向北增生、碰撞以及燕山期伊佐奈岐板塊的俯沖，盆地西緣北段的響應顯示為陸內前陸盆地的特徵。
  17. Situated at the both e w sides of pamir, the s w tarim and tadjik basins have the similar evolution history of tectono sedimentary processes during cenozoic, i. e. steady subsidence with transgressive sequence in paleogene and speedy subsidence with continental molassetype sediments in strong compressive tectonic environment in neogene - quaternery. since neogene, for the effect of pamir and west kunlun s northward moving and thrusting, there is complicated tectonostructural deformation taking place in tadjik and sw tarim. neogene stratigraphic combination and later structural deformation of tadjik basin and southwestern tarim much resemble each other in terms of extent of transpressional processes. paleogene in tadjik basin is main oil - bearing sequence and many substantial oil - gas fields there have been found. so, it can be assured in comparison that there is oil - gas perspective also in southwestern tarim region

    第四紀受強烈擠壓快速沉降接受陸相磨拉石沉積。自新第三紀以來，受帕米爾西昆侖北移和隆升沖斷的影響，塔西南和塔吉克盆地發生了復雜的褶皺沖斷變形，其差異在於塔西南明顯地受走滑為主的剪壓構造作用，而塔吉克盆地是受擠壓為主的剪壓構造作用的影響。塔西南和塔吉克盆地下第三系巖相組合類似，後期構造變形也相似，塔吉克盆地下第三系是該盆地的主力油層，已有許多油氣田發現，因此可以推斷塔西南也應該有良好的油氣前景。
  18. According to the basic principle of sedimentary geochemistry, two geochemical sections from dongying sag of bohai bay region and turpan basin were selected as the standard models of deep - water rift - subsidence basin and shallow water coal measure basin, respectively

    結果表明，該盆地侏羅系地層元素特徵與東營凹陷很相似，由此推知其古環境在更大程度上傾向于東部深水斷陷湖盆。
  19. Based on the basic geology this paper determines the development history of kailu basin, and comprehensively analyses hydrogeologic conditions and hydrogeochemical characteristics, as well as the uranium concentration in groundwater, determines the prospecting significance of regional confined aquifers in yaojia and sifangtai formations formed during the subsidence stage of the basin

    本文從基礎地質條件出發，界定了開魯盆地的發展歷史，全面分析了研究區的水文地質條件、水文地球化學特徵及地下水的含鈾性，確定了在整體坳陷期形成的姚家組和四方臺組區域承壓含水層的找礦意義。
  20. The maximal depth of source rock in china is distributed in 3000 - 4000 metres, the average subsidence rate of a basin is no more than 100 metres each million year, and maximal subsidence rate is more than 300 metres each million year ; the uplift rate is also no more than 100 metres each million year, and maximal uplift rate is more than 300 metres each million year, the maximal degradation thickness is more than 2000 metres

    中國含油氣盆地烴源巖最大埋深主要分佈在3000 - 4000m 。盆地沉降速率一般在100m / ma的范圍內，最大可達300m / ma ；經歷抬升型盆地抬升剝蝕速率一般在100m / ma的范圍內，最大也可達300m / ma ，剝蝕厚度最大可大於2000m 。
分享友人
分享到 Line

分享到臉書